Subsidence is the downward settling of the ground due to natural or human caused processes. A few natural processes include the thawing of permafrost, normal faulting, and the oxidation of organic soils. Human activities that result in subsidence are the extraction of natural gas, water,and petroleum, as well as mining. Parts of Colorado Springs have experienced subsidence due to a series of shallow, abandoned mines.
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OF-12-02 Colorado Map of Potential Evaporite Dissolution and Evaporite Karst Subsidence Hazards
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IS-22 Annotated Bibliography of Subsidence Studies over Abandoned Coal Mines in Colorado [2010 update]
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RockTalk: Colorado Geological Survey – 2007 Summary
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MS-47 Collapsible Soil Susceptibility Map of the Colorado River Corridor in the Vicinity of Rifle, Garfield County, Colorado
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RockTalk: Annual Review 2005
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RockTalk: Colorado Coal
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MS-34 Collapsible Soils and Evaporite Karst Hazards of the Roaring Fork River Corridor, Garfield, Eagle, and Pitkin Counties, Colorado
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RockTalk: Ground Subsidence and Settlement Hazards
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OF-87-03 Tri-Towns Subsidence Investigation, Weld County, Colorado
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SP-31 Proceedings of the 1985 Conference on Coal Mine Subsidence in the Rocky Mountain Region
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SP-26 Subsidence above Inactive Coal Mines: Information for the Homeowner
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MI-27 Geology of Denver, Colorado, U.S.A.
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EG-09 Coal Mine Subsidence and Land Use in the Boulder-Weld Coalfield: Boulder and Weld Counties, Colorado
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